2) paleo-uplift
古隆起
1.
Accumulation and distribution of oil and gas controlled by paleo-uplift in poly-history superimposed basin;
多期叠加盆地古隆起控油规律
2.
Formation mechanism and tectonic types of intracratonic paleo-uplifts in the Tarim basin;
塔里木盆地克拉通内古隆起的成因机制与构造类型
3.
The Research on Ordovician Sedimentology and Reservoir Property of Leshan～Longnvsi Paleo-uplift in Centre Sichuan Area;
川中地区乐山～龙女寺古隆起奥陶系沉积、储层特征研究
3) paleohigh
古隆起
1.
Petroleum controlling theory of Lunnan paleohigh and its buried hill pool exploration technology,Tarim Basin;
轮南古隆起控油理论及其潜山准层状油气藏勘探
2.
Formation,Evolution and Hydrocarbon-Controlling Geological Conditions of Major Paleohighs,Tarim Basin;
塔里木盆地主要古隆起的形成、演化及控油气地质条件分析
3.
The Three Main Paleohigh's Evolution and Affection Hydrocarbon Accumulation, Tarim Basin
塔里木盆地三大控油古隆起形成演化与油气成藏关系研究
4) palaeouplift
古隆起
1.
It was the deep fracture and palaeouplift developed before deposition of lower Xingouzui formation that visibly controlle.
研究了江汉盆地潜江凹陷东南部地区构造演化、沉积体系类型及其沉积相模式、沉积体系展布及其控制因素,分析认为潜江凹陷东南部地区新沟嘴组下段主要发育三角洲-咸水湖泊沉积体系,新沟嘴组下段沉积之前发育的深大断裂、继承性古隆起对新沟嘴组下段沉积相展布具有明显的控制作用。
2.
This paper discusses the oil-control effect of the paleaouplift by analyzing structural evolution feature of the palaeouplift early Hercynian period in Tarim Basin.
通过塔里木盆地海西早期古隆起的构造演化特征分析,探讨了古隆起的控油作用。
5) palaeohigh
古隆起
1.
Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei palaeohighs in Tarim Basin;
塔中、塔北古隆起形成演化及油气地质条件对比
2.
The palaeohigh in Junggar basin underwent multistage evolution from Neopaleozoic to Cenozoic, and four basic types such as successional, discontinuous, tilted and thrust ones were developed.
准噶尔盆地古隆起经历了自晚古生代至新生代的多期次演化,发育了继承型、间断型、掀斜型和冲断带型等4种古隆起基本类型,通过构造沉积演化及油气成藏分析探讨了陆梁隆起、莫索湾凸起、车莫隆起的油气勘探领域和勘探方向。
3.
The foreland basins are the oil and gas abundance zones while the palaeohighs control the large-scale oil and gas accumulation.
任何大盆地的形成、发生和发展都离不开区域构造背景,全球的油气分布与几个大构造带有紧密关系,前陆盆地是油气的富集区,古隆起控制着大规模油气聚集。
6) paleouplift
古隆起
1.
As the paleouplifts in the south of China have been reconstructed in different degrees, the intact uplifting faces do not ex.
南方古隆起均被不同程度地改造,使完整的隆起面貌已不复存在。
2.
limestone reservoirs and dolomite reservoirs,are developed at Hetian Paleouplift area.
塔里木盆地和田古隆起区下古生界发育灰岩、白云岩两类储层。
3.
The study on the sedimentary filling and evolution in and around Jianghan Plain indicated that the Sinian-Lower Paleozoic source rocks and reservoirs in Jianghan Plain were controlled by the Caledonian paleouplift.
通过对江汉平原及周缘沉积充填演化研究表明,江汉平原加里东期古隆起控制了震旦系—下古生界烃源岩、储层的分布。
补充资料：大兴隆起
北京活动构造带。斜贯北京小平原中部，呈北东走向，隐伏于地表之下。面积约为1300平方公里。大兴区域大部处于隆起的中部。其西北侧为北京凹陷，东南侧为燕郊－牛堡屯断裂、大厂凹陷，两侧分别以南苑－通州断裂带及永乐店－夏垫－马坊断裂带为界。南段与南各庄－长子营断裂、廊固凹陷为邻。隆起西北高而东南低，高点埋深仅几十米，位于黄村镇与南苑镇之间，形成于第三纪，上覆50～1000米左右的第三系和第四系地层，内幕是由中上元古界和古生界组成的蓟县系、青白口系、寒武系、奥陶系地层。次级背斜轴部在高点东向，约在榆垡－马驹桥一线。新生界地层由西北向东南逐渐加厚。大兴隆起的两侧有次一级的断裂下降活动，与北京凹陷相应，形成地垒式的构造。隆起的上部地表呈平原地貌形态。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条